Articles | Volume 9, issue 2
https://doi.org/10.5194/essd-9-639-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/essd-9-639-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Global Inventory of Gas Geochemistry Data from Fossil Fuel, Microbial and Burning Sources, version 2017
Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado, 80303, USA
Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia, B3H 4R2, Canada
Stefan Schwietzke
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, 80303, USA
NOAA Earth System Research Laboratory, Global Monitoring Division, Boulder, Colorado, 80305, USA
Victoria A. Arling
NOAA Earth System Research Laboratory, Global Monitoring Division, Boulder, Colorado, 80305, USA
Giuseppe Etiope
Istituto Nazionale di Geofisica e Vulcanologia, Rome, 00143, Italy
Faculty of Environmental Science and Engineering, Babes-Bolyai University, Cluj-Napoca, 400294, Romania
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- Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources B. Riddell-Young et al. 10.1038/s41561-023-01332-x
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Short summary
Multiple natural and anthropogenic emissions sources contribute to the global atmospheric methane budget. Methane emissions are constrained, in part, by inverse (top-down) models that incorporate data on the concentration and stable carbon and hydrogen isotopic ratios of methane from different sources. To aid in these modeling efforts, we present a geochemical database comprising over 10 000 discrete samples from fossil and non-fossil fuel sources of methane.
Multiple natural and anthropogenic emissions sources contribute to the global atmospheric...
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